Inastronomy, therotation period orspin period[1] of acelestial object (e.g., star, planet, moon, asteroid) has two definitions. The first one corresponds to thesidereal rotation period (orsidereal day), i.e., the time that the object takes to complete afull rotation around itsaxis relative to the background stars (inertial space). The other type of commonly used "rotation period" is the object'ssynodic rotation period (orsolar day), which may differ, by a fraction of a rotation or more than one rotation, to accommodate the portion of the object'sorbital period around a star or another body during one day.
For solid objects, such as rockyplanets andasteroids, the rotation period is a single value. For gaseous or fluid bodies, such asstars andgiant planets, the period of rotation varies from the object's equator to itspole due to a phenomenon calleddifferential rotation. Typically, the stated rotation period for a giant planet (such as Jupiter, Saturn, Uranus, Neptune) is its internal rotation period, as determined from the rotation of the planet'smagnetic field. For objects that are notsphericallysymmetrical, the rotation period is, in general, not fixed, even in the absence ofgravitational ortidal forces. This is because, although the rotation axis is fixed in space (by theconservation of angular momentum), it is not necessarily fixed in the body of the object itself.[citation needed] As a result of this, themoment of inertia of the object around the rotation axis can vary, and hence the rate of rotation can vary (because the product of the moment of inertia and the rate of rotation is equal to the angular momentum, which is fixed). For example,Hyperion, a moon ofSaturn, exhibits this behaviour, and its rotation period is described aschaotic.
^abcThis rotation is negative because the pole which points north of theinvariable plane rotates in the opposite direction to most other planets.
^Reference adds about 1 ms to Earth's stellar day given in mean solar time to account for the length of Earth's mean solar day in excess of 86400 SI seconds.
^abRotation period of the deep interior is that of the planet's magnetic field.
^T. A. Hromakina; I. N. Belskaya; Yu. N. Krugly; V. G. Shevchenko; J. L. Ortiz; P. Santos-Sanz; R. Duffard; N. Morales; A. Thirouin; R. Ya. Inasaridze; V. R. Ayvazian; V. T. Zhuzhunadze; D. Perna; V. V. Rumyantsev; I. V. Reva; A. V. Serebryanskiy; A. V. Sergeyev; I. E. Molotov; V. A. Voropaev; S. F. Velichko (2019-04-09). "Long-term photometric monitoring of the dwarf planet (136472) Makemake".Astronomy & Astrophysics.625: A46.arXiv:1904.03679.Bibcode:2019A&A...625A..46H.doi:10.1051/0004-6361/201935274.S2CID102350991.